This document discusses factors that influence grape growing conditions such as climate, geology, and soils. It provides information on the relative cold hardiness and heat requirements of different grape varieties. It also describes how geological materials and processes form the basis for soil development over long periods of time. Specific geological events that shaped soils in the Columbia Basin region are outlined. Key properties of soils important for wine grapes, such as depth, texture, drainage, and mineral content are also summarized.
1. Introduction to Vines and Wines
Hort/VE 113 Fall 2012
Session 6 -Grape Growing:
climate and environment(cont.) Geology and Soils
Relative Cold Hardiness
Low Moderate High
Chenin blanc Sauvignon Riesling
blanc
Merlot Lemberger Chardonnay
Sangiovese Cabernet Gewurztraminer
sauvignon
Semillon Cabernet Pinot noir
franc
Syrah Pinot gris
Viognier Pinot blanc
Relative Heat Requirements
Low Moderate High
Riesling Chardonnay Sauvignon blanc
Gewurztraminer Lemberger Cabernet franc
Pinot noir Merlot Semillon
Pinot blanc Syrah Cabernet sauvignon
Pinot gris Sangiovese
Chenin blanc
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2. http://www.youtube.com/wa
tch?v=sVaZFCzxx24&playn
ext=1&list=PLAC8CA53A2E
20D3DD&feature=results_vi
deo
Geology vs Soil
• Geology • Soil
• Study of the Earth • A natural body comprised
of solids (minerals and
• The materials of which it organic matter), liquid, and
is made gases
• The structure of those • Occurs on the land surface
materials • Has horizons, or layers,
• and the processes acting that are distinguishable
upon them from the parent material
• As a result of additions,
losses, transfers, and
transformations
Geologic materials and processes
are the building blocks upon which
soils are formed
Vineyards grow on soils
Soils influence grape yield and
quality
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4. Metamorphic Rocks
SOIL FORMATION
Geologic materials
on
Landscapes
are weathered by
Climate
under i fl
d influence of
f
Vegetation
over eons of
Time
to form
Soils
GEOLOGY AND SOILS
Courtesy of:
Joan Davenport
Soil Scientist
WSU-Prosser
jdavenp@wsu.edu
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5. Where in the
World?
Unique Pleistocene History of
Columbia Basin
Event Result
Episodes of Glaciation Sculpting of W. Canada &
PNW US; bouldery soil
materials
Unique Pleistocene History of
Columbia Basin
Event Result
Episodes of Glaciation Sculpting of W. Canada
& PNW US; bouldery soil
materials
“Cataclysmic” Glacial Channeled Scabland
Outburst Floods
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6. Unique Pleistocene History of
Columbia Basin
Event Result
Episodes of Glaciation Sculpting of W. Canada
& PNW US; bouldery soil
materials
“Cataclysmic” Glacial Channeled Scabland
Outburst Floods
Strong Directional Dune fields and Palouse
Winds loess
Unique Pleistocene History of
Columbia Basin
Event Result
Episodes of Glaciation Sculpting of W. Canada
& PNW US; bouldery soil
materials
“Cataclysmic” Glacial Channeled Scabland
Outburst Floods
Strong Directional Dune fields and Palouse
Winds loess
High Cascades; ash
Volcanic Eruptions added to soils
Glaciation
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15. Generalized Soil Properties Important for
Wine Grape
• Depth
• Texture & Structure
• Available water holding capacity
• Drainage
• Chemical Properties
• Quality (om, biota)
• Spatial variability
Soil Depth
•Important for root zone
•depth of root penetration
•water holding capacity
d
•drainage
•nutrient holding capacity
Site Potential (R. Smart)
• Based on depth of potential root zone
• high > 1m
• medium 0.5
05-1m
• low < 0.5 m
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16. Soil Texture
• % Sand (S)
0.05 - 2.0 mm
• % Silt (Si)
0.002 - 0.05 mm
• % Clay (C)
< 0.002 mm
Soil Texture
• % Sand (S)
0.05 - 2.0 mm
• % Silt (Si)
0.002 0.05
0 002 - 0 05 mm
• % Clay (C)
< 0.002 mm
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17. Soil Textural Gradient
In general, soils
in central WA
are sandy close
to the i
t th river and d
become more fine
when moving
inland.
Soil as a three phase system
liquid gas
solid
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18. void
gas liquid
solid solid
VOIDS (Pores)
•Macropores
•mostly air
•Micropores
•mostly water
l
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19. Soils
•Well drained generally best
•Mixtures of sand, gravel, organic matter
•Drainage can be improved with drainage
tile
til
•Many wines benefit from the mineral
content of the soil– sometimes chalky
•Rootstocks are selected for soil
characteristics (texture, pH)
Thank you Dr. Davenport!
• http://wine.wsu.edu/faculty/joan-davenport
• /
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